Skip to content

Bennett Beach Sand Dunes EarthCache

Hidden : 5/2/2007
Difficulty:
1.5 out of 5
Terrain:
2.5 out of 5

Size: Size:   not chosen (not chosen)

Join now to view geocache location details. It's free!

Watch

How Geocaching Works

Related Web Page

Please note Use of geocaching.com services is subject to the terms and conditions in our disclaimer.

Geocache Description:

Bennett Beach is along the shores of Lake Erie in Evans, NY. The beach is operated by the Erie County Parks Dept. Along with the geological feature of the sand dunes, the park also offers picnicking, swimming, fishing and great sunsets.

Roughly speaking, sand dunes are large hills of sand that result when wind or water carried sand particles accumulate. Coastal dunes protect the landscape behind them from wind and waves, and provide a substrate, or ground, for plants to form communities upon. The dunes at Bennett Beach also provide habitat for various birds such as ducks, gulls and heron. Estimates are that the dunes at Bennett Beach are between 3,000 and 4,000 years old, as are many of the dunes along the Great Lakes. Three things are required for dune formation to occur: a large supply of sand, wind speeds capable of moving it, and a location for sand to accumulate. Sand is composed of particles of eroded rock material varying in size from 0.02 mm to 1.6 mm. Most of the rock material that is eroded into sand is done so either by water or ice. As the sand is washed ashore by waves and currents, the wind begins to propel the sand particles via either airborne suspension in the wind or saltation. Saltation is the bouncing of sand particles by wind along the ground. The majority of sand moved into dunes is done by saltation. As these particles move forward they also bump other particles forward, which is known as surface creeping. The moving sand either stops when the wind subsides below approximately 10 mph or the sand meets an obstruction. Common obstructions include trees, vegetation, rocks and animal carcasses. A small mound called a hummock is then formed. Once the hummock is formed, the wind continues to move the sand up the pile. Once the pile becomes too steep it collapses on itself and the excess sand falls down the leeward side or slip face of the dune. The collapsing sand comes to rest when it reaches just the right steepness to keep the dune stable which is usually on an incline of 30 to 34 degrees. As this process repeats itself, the sand dune grows.



The logging requirements for this Earthcache are:
1. Post a picture of the dunes at Bennett Beach with your log entry.
2. Report the wind speed and wave height when you visited the dunes in your log entry. Both estimations or actual meteorological data are acceptable.
3. Measure or estimate the height of the sand dunes and e-mail me your results.


Please provide me with any feedback which will make this Eartcache more enjoyable. Thanks!

Congrats to Detecto on the FTF!

Additional Hints (Decrypt)

Vg'f nyzbfg vzcbffvoyr gb xrrc vg bhg bs lbhe fubrf.

Decryption Key

A|B|C|D|E|F|G|H|I|J|K|L|M
-------------------------
N|O|P|Q|R|S|T|U|V|W|X|Y|Z

(letter above equals below, and vice versa)